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Global Volcanism Program | Image GVP-07393

Cerro El Chino is seen here from the east, just south of the town of Aguilares and is part of the Cerro Cinotepeque volcanic field, a large group of small Pleistocene-to-Holocene stratovolcanoes and cones constructed along NW-SE-trending faults on either side of the Río Lempa west of Guazapa volcano. The Holocene Cerro Cinotepeque cone lies about 6 km NW of Cerro El Chino. Photo by Giuseppina Kysar, 1999 (Smithsonian Institution).

Cerro El Chino is seen here from the east, just south of the town of Aguilares and is part of the Cerro Cinotepeque volcanic field, a large group of small Pleistocene-to-Holocene stratovolcanoes and cones constructed along NW-SE-trending faults on either side of the Río Lempa west of Guazapa volcano. The Holocene Cerro Cinotepeque cone lies about 6 km NW of Cerro El Chino.

Photo by Giuseppina Kysar, 1999 (Smithsonian Institution).

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Cerro Cinotepeque